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Studies have suggested that NO−2, produced during nitrification and denitrification, can become incorporated into soil organic matter and, in one of the processes associated with chemodenitrification, react with organic matter to form trace N gases, including N2O. To gain an understanding of the nitrosation chemistry on a molecular level, soil and aquatic humic substances were reacted with 15N‐labeled NaNO2, and analyzed by liquid phase 15N and 13C nuclear magnetic resonance (NMR). The International Humic Substances Society (IHSS) Pahokee peat and peat humic acid were also reacted with Na15NO2 and analyzed by solid‐state 15N NMR. In Suwannee River, Armadale, and Laurentian fulvic acids, phenolic rings and activated methylene groups underwent nitrosation to form nitrosophenols (quinone monoximes) and ketoximes, respectively. The oximes underwent Beckmann rearrangements to 2° amides, and Beckmann fragmentations to nitriles. The nitriles in turn underwent hydrolysis to 1° amides. Peaks tentatively identified as imine, indophenol, or azoxybenzene nitrogens were clearly present in spectra of samples nitrosated at pH 6 but diminished at pH 3. The 15N NMR spectrum of the peat humic acid exhibited peaks corresponding with N‐nitroso groups in addition to nitrosophenols, ketoximes, and secondary Beckmann reaction products. Formation of N‐nitroso groups was more significant in the whole peat compared with the peat humic acid. Carbon‐13 NMR analyses also indicated the occurrence of nitrosative demethoxylation in peat and soil humic acids. Reaction of 15N‐NH3 fixated fulvic acid with unlabeled NO−2 resulted in nitrosative deamination of aminohydroquinone N, suggesting a previously unrecognized pathway for production of N2 gas in soils fertilized with NH3

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~~~~~ ~ rn Suwannee River fulvic acid was reacted with aqueous solutions of 15N-labeled chloramine and 15N-labeled ammonia. INEPT 15N-NMR spectra of the lyophilized products from both reactions exhibit major resonances between 90 and 120 ppm, denoting the formation of amides, enaminones, and/or aminoquinones. The striking similarity between spectra suggests that the observed N moieties result from reactions between fulvic acid and ammonia, an expected coproduct from the chlorination of the fulvic acid by Chloramine. This represents the first evidence for the formation of N-containing compounds from the chloramination of dissolved organic matter in natural waters. 1954,26, 1388.